Mediterranean climate

Mediterranean Climate

Mediterranean climate (pronunciation: /ˌmɛdɪtəˈreɪniən ˈklaɪmɪt/) is a type of climate characterized by dry summers and mild, wet winters. The term "Mediterranean" refers to the regions around the Mediterranean Sea where this type of climate is most common, but it can be found in other parts of the world as well.

Etymology

The term "Mediterranean climate" comes from the Latin words "medius" (middle) and "terra" (land), referring to the land around the Mediterranean Sea. The term was first used in the 19th century to describe the climate of these regions.

Characteristics

Mediterranean climates are characterized by hot, dry summers and mild, wet winters. The summer months are typically dry due to the presence of a high-pressure system, while the winter months are wet due to the presence of a low-pressure system. The temperature in a Mediterranean climate typically ranges from 30 to 50 degrees Fahrenheit in the winter and 70 to 90 degrees Fahrenheit in the summer.

Regions with Mediterranean Climate

Regions with a Mediterranean climate include the Mediterranean Basin, parts of western and southern Australia, western North America, and parts of central Chile. These regions are typically located on the western coasts of continents, between 30 and 40 degrees latitude.

Related Terms

Köppen climate classification: A system for classifying the world's climates, developed by German climatologist Wladimir Köppen. Mediterranean climate is classified as "Csa" or "Csb" in this system.
Mediterranean Sea: The sea surrounded by the Mediterranean region, after which the Mediterranean climate is named.
Mediterranean Basin: The region around the Mediterranean Sea that has a Mediterranean climate.
Mediterranean vegetation: The types of plants that are adapted to the conditions of a Mediterranean climate, such as olive trees and grapevines.